Estimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert survey

dc.bibliographicCitation.firstPage18eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.journalTitlenpj Climate and Atmospheric Scienceeng
dc.bibliographicCitation.volume3eng
dc.contributor.authorHorton, Benjamin P.
dc.contributor.authorKhan, Nicole S.
dc.contributor.authorCahill, Niamh
dc.contributor.authorLee, Janice S. H.
dc.contributor.authorShaw, Timothy A.
dc.contributor.authorGarner, Andra J.
dc.contributor.authorKemp, Andrew C.
dc.contributor.authorEngelhart, Simon E.
dc.contributor.authorRahmstorf, Stefan
dc.date.accessioned2021-11-29T08:51:27Z
dc.date.available2021-11-29T08:51:27Z
dc.date.issued2020
dc.description.abstractSea-level rise projections and knowledge of their uncertainties are vital to make informed mitigation and adaptation decisions. To elicit projections from members of the scientific community regarding future global mean sea-level (GMSL) rise, we repeated a survey originally conducted five years ago. Under Representative Concentration Pathway (RCP) 2.6, 106 experts projected a likely (central 66% probability) GMSL rise of 0.30–0.65 m by 2100, and 0.54–2.15 m by 2300, relative to 1986–2005. Under RCP 8.5, the same experts projected a likely GMSL rise of 0.63–1.32 m by 2100, and 1.67–5.61 m by 2300. Expert projections for 2100 are similar to those from the original survey, although the projection for 2300 has extended tails and is higher than the original survey. Experts give a likelihood of 42% (original survey) and 45% (current survey) that under the high-emissions scenario GMSL rise will exceed the upper bound (0.98 m) of the likely range estimated by the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, which is considered to have an exceedance likelihood of 17%. Responses to open-ended questions suggest that the increases in upper-end estimates and uncertainties arose from recent influential studies about the impact of marine ice cliff instability on the meltwater contribution to GMSL rise from the Antarctic Ice Sheet. © 2020, The Author(s).eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/7541
dc.identifier.urihttps://doi.org/10.34657/6588
dc.language.isoengeng
dc.publisherLondon : Springer Natureeng
dc.relation.doihttps://doi.org/10.1038/s41612-020-0121-5
dc.relation.essn2397-3722
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc333.7eng
dc.subject.ddc530eng
dc.subject.otherSea-level rise projectionseng
dc.subject.otherglobal mean sea-level (GMSL)eng
dc.subject.otherclimate changeeng
dc.titleEstimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert surveyeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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